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    Some Characteristic Features of Hygroscopic and Non-Hygroscopic Aerosols at Delhi

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 006::page 771
    Author:
    Sekhon, R. S.
    ,
    Murty, B. H. V. Ramana
    DOI: 10.1175/1520-0469(1966)023<0771:SCFOHA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The concentrations of hygroscopic and non-hygroscopic aerosols in large and giant size ranges were measured at Delhi in different periods during 1960?62. The content of ice-forming aerosols also was estimated simultaneously for brief periods. Observations made during the monsoon season showed marked variations in the content of hygroscopic particulate matter during the day. The content of non-hygroscopic component also showed significant variation from one day to another. The average level of the hygroscopic component is found to rise conspicuously with the amount of rainfall received, while that of the non-hygroscopic component is seen to decrease. Parallel measurements on hygroscopic and ice-forming nuclei suggest that some of the hygroscopic aerosols of oceanic origin might possess ice-nucleating properties.
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      Some Characteristic Features of Hygroscopic and Non-Hygroscopic Aerosols at Delhi

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4150919
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    contributor authorSekhon, R. S.
    contributor authorMurty, B. H. V. Ramana
    date accessioned2017-06-09T14:13:57Z
    date available2017-06-09T14:13:57Z
    date copyright1966/11/01
    date issued1966
    identifier issn0022-4928
    identifier otherams-15266.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150919
    description abstractThe concentrations of hygroscopic and non-hygroscopic aerosols in large and giant size ranges were measured at Delhi in different periods during 1960?62. The content of ice-forming aerosols also was estimated simultaneously for brief periods. Observations made during the monsoon season showed marked variations in the content of hygroscopic particulate matter during the day. The content of non-hygroscopic component also showed significant variation from one day to another. The average level of the hygroscopic component is found to rise conspicuously with the amount of rainfall received, while that of the non-hygroscopic component is seen to decrease. Parallel measurements on hygroscopic and ice-forming nuclei suggest that some of the hygroscopic aerosols of oceanic origin might possess ice-nucleating properties.
    publisherAmerican Meteorological Society
    titleSome Characteristic Features of Hygroscopic and Non-Hygroscopic Aerosols at Delhi
    typeJournal Paper
    journal volume23
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1966)023<0771:SCFOHA>2.0.CO;2
    journal fristpage771
    journal lastpage777
    treeJournal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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